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Warming impacts on carbon, nitrogen and phosphorus distribution in soil water-stable aggregates

机译:变暖对土壤水稳性团聚体中碳,氮和磷分布的影响

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A five-year (2010–2015) field experiment was conducted to investigate warming impacts on organic carbon (OC), total nitrogen (TN) and total phosphorus (TP) contents and their ratios in bulk soil and soil water-stable aggregates in an alpine meadow of the Tibetan Plateau. Compared with unwarmed control, warming had no significant effects on OC, TN and TP contents and their ratios in bulk soil. The contents of OC, TN and TP associated with macroaggregates and microaggregates decreased, whereas those associated with silt + clay fractions significantly increased. The C:N and C:P ratios in macro- and microaggregates and silt + clay fractions decreased, with significant differences for C:P ratio in microaggregates and C:N and C:P ratios in silt + clay fractions. The results indicated that C, N and P were protected chemically in silt- and clay-size fractions under warming, which offset the loss of C, N and P protected physically by macro- and microaggregates. Both physically and chemically protected C decomposition proceeded relatively more rapidly or accumulated relatively more slowly than did N and P. Our results suggest that C, N and P distributions within soil aggregate size fractions influence their net changes in bulk soil under future climate change scenarios.
机译:进行了为期五年(2010-2015年)的田间试验,研究了变暖对土壤中整块土壤和水稳性团聚体中有机碳(OC),总氮(TN)和总磷(TP)含量及其比例的影响。青藏高原的高山草甸。与未保温相比,变暖对散装土壤中的OC,TN和TP含量及其比例没有显着影响。与大骨料和微骨料有关的OC,TN和TP含量下降,而与粉土和粘土碎屑有关的含量显着增加。大团聚体和微团聚体中的C:N和C:P比值降低了,而粉尘+黏土组分中的比例降低了,而微团聚体中的C:P比值和粉砂+黏土组分中的C:N和C:P值差异显着。结果表明,C,N和P在变暖的粉砂和粘土大小馏分中受到化学保护,从而抵消了由大骨料和微骨料物理保护的C,N和P的损失。在物理和化学保护下,碳的分解均比氮和磷的分解进行得相对快或慢。我们的研究结果表明,在未来气候变化情景下,土壤团聚体中碳,氮和磷的分布会影响其在大块土壤中的净变化。

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